200 BCE.
a tool used by scientists to measure earthquakes by movement
A seismograph is the device that scientists use to measure earthquakes. The goal of a seismograph is to accurately record the motion of the ground during a quake
A seismograph records earthquake waves.the correct answer is a seismometer a seismograph is the graph to show the recordings
Seismometers are devices used to record seismic waves generated by earthquakes. These waves can provide valuable information about the earthquake's location, magnitude, and depth, helping scientists better understand and study seismic events.
That would be a seismometer. (size-MOM-uh-ter)
The ancient culture that kept records of earthquakes as early as 780 BCE is the ancient Chinese culture. They documented earthquakes for centuries in their historical records.
a tool used by scientists to measure earthquakes by movement
The historical record of earthquakes is very slim. Earthquakes happened thousands of years before man began keeping records. There are some historical evidence of past earthquakes and the ruins they left so they did happen. No one can tell you when the first one happened.
refence from books of impact of poor records keeping
Seismograph
It is important for scientists to keep records to ensure reproducibility and transparency in their research. Keeping detailed records allows other researchers to verify findings and build on previous work. It also helps scientists track their progress, identify errors, and comply with regulations and ethical standards.
it records the magnitude of earthquakes.
Earthquakes
Scientists must keep accurate records to ensure the reproducibility and validity of their work. Accurate records allow others to verify their findings and build upon their research. It also helps prevent errors and biases in data collection and analysis.
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keeping records of their whereabouts.
Scientists found that earthquakes are not randomly distributed; instead, they occur along specific tectonic plate boundaries. This led to the development of the theory of plate tectonics, which explains how the Earth's lithosphere is divided into several large plates that are constantly moving and interacting with each other. The majority of earthquakes occur at these plate boundaries where tectonic forces create stress and lead to seismic activity.